Recurrent marine anoxia in the Paleo-Tethys linked to constriction of seaways during the Early Triassic-Reference-Cited by-同舟云学术

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Recurrent marine anoxia in the Paleo-Tethys linked to constriction of seaways during the Early Triassic

Published:2024-10 Issue: Volume:643 Page:118882
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Wu Yuyang^ORCID,Pohl Alexandre^ORCID,Tian Li,Corso Jacopo Dal^ORCID,Cui Ying,Chu Daoliang,Tong Jinnan,Song Huyue,Song Hanchen,Song Haijun^ORCID

Publisher

Elsevier BV

Reference60 articles.

1. The Early Triassic ammonoid recovery: paleoclimatic significance of diversity gradients;Brayard;Paleogeogr. Paleoclimatol. Paleoecol.,2006

2. Smithian and Spathian (Early Triassic) ammonoid assemblages from terranes: paleoceanographic and paleogeographic implications;Brayard;J. Asian Earth Sci.,2009

3. Rapid expansion of oceanic anoxia immediately before the end-Permian mass extinction;Brennecka;Proc. Natl. Acad. Sci. USA,2011

4. Initial pulse of Siberian Traps sills as the trigger of the end-Permian mass extinction;Burgess;Nat. Commun.,2017

5. The timing and pattern of biotic recovery following the end-Permian mass extinction;Chen;Nat. Geosci.,2012

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